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Atmospheric CO2 changes since the last glacial maximum: evidence from the stomatal density record of fossil leaves

โœ Scribed by David J. Beerling; William G. Chaloner


Book ID
116054677
Publisher
Elsevier Science
Year
1994
Tongue
English
Weight
530 KB
Volume
81
Category
Article
ISSN
0034-6667

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The Younger Dryas stadia1 (1 1 000-10000 yr BP) was an abrupt return to a glacial climate during the termination of the last glaciation. We have reconstructed atmospheric CO, concentrations from a high-resolution sequence of fossil Salix herbacea leaves through this climatic oscillation from Kriiken